松辽盆地徐家围子断陷火山活动期次与烃源岩演化

doi:10.11743/ogg20050314

Abstract

Abstract:

Xujiaweizi fault depression has experienced three relatively large volcanic activities during rift fauting,among which the volcanic activity duing the deposition of Yingcheng Fm had the longest duration.The volcanic activity speeded up the maturation of the major source rocks including deep Huoshiling Fm,Shahezi Fm and Yingcheng Fm. Simulations of burial history,thermal history and hydrocarbon generation history show that the R_o value of Huoshiling Fm source rocks at a burial depth of 1300m would have rapidly reached 0.7% in about 1Ma.The R_o value of Shahezi and Huoshiling Fins source rocks would have reached 1% at a burial depth of 2600m.Before the deposition of Quantou Fm,Shahezi and Huoshiling Fins source rocks would have entered the peak of gas generation.Before the deposition of Qingshankou Fro,Yingcheng Fin source rocks would have been in the peak of gas generation,while Shahezi and Huoshiling Fms source rocks would have begun to generate dry gas.At this time,the regional seals of the 2^ndmember of Denglouku Fm and the 1^st and 2^nd members of Quantou Fm would have been formed,leading to the formation of gas pools in Yingcheng-Quantou Fms.By the end of the deposition of Nenjiang Fm,the movement of boundary faults led to the redistribution of gas pools in Yingcheng-Quantou Fms.

Key words: source rock, hydrocarbon generation history, natural gas, deep formations in Songliao basin

CLC Number:

TE112.3

Jin Xiaohui, Lin Renzi, Zhou Huayao, Feng Zihui, Ren Yanguang. Volcanic activities and evolution of source rocks in Xujiaweizi fault depression, Songliao basin[J]. Oil & Gas Geology, 2005, 26(3): 349-355.

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Volcanic activities and evolution of source rocks in Xujiaweizi fault depression, Songliao basin

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